摘要
广西司律铅锌矿矿体呈似层状、透镜状,均分布于次级的层间断层破碎带中,矿体围岩以下泥盆统上伦组(D_1sl)白云岩、泥质灰岩为主。该矿床属热液充填(交代型铅锌矿床。
The ore body of Silu Pb-Zn deposit in Guangxi is stratoid,lenticular in the secondary interlayer fault. The main wall rock is Lower Devonian Shanglun Formation( D_1sl) dolomitite,muddy limestone. It belongs to the hydrothermal filling( metasomatism) Pb-Zn deposit.
引文
[1]翟裕生,姚书振,蔡克勤等.矿床学[M].北京:地质出版社,2011,1-417.
[2]方科,曾南石,王谦,牛聪聪.大瑶山西侧中下泥盆统白云岩岩石学及有序度特征研究[J].矿物学报,2011(1):766-767.
[3]广西地质矿产局.广西泥盆纪沉积相古地理及矿产[M].南宁:广西人民出版社,1987.